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THE ORDOVICIAN CARBONIC RESERVOIR CHARACTERISTICS AND MINERALIZATION IN YINGMAILI LOW HEAVE OF TARIM BASIN
塔里木盆地英买力低凸起奥陶系碳酸盐岩储层特征及其成岩作用

Keywords: Tarim basin,Yingmaili low heave,Ordovician,Carbonic reservoir characteristics,Diagenesis
塔里木盆地
,英买力凸起,奥陶系,碳酸盐岩储层特征,成岩作用

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Abstract:

The yingmail low heave carbonic buried hill includes gray,dark-gray,offwhite and dust-colour biologic,sandstonic,strumae,mud carbonate And dolomite.It is separated eight lithology sects from up to down:Mud carbonate,gray matter mud, strumaed carbnote,biologic carbnote,flint carbnote,mud and biologic carbonate,dolomitic carbnote,carbnotic dolonate.It is separated five mineralization types:exposure bank,harst,deep buried dolomite,paleo-carbonate buried hill,tectonic-rimose and so on.In the long geologic evolvement,it lived seawater mineralization condition,mixed water mineralization condition,vaporized seawater mineralization condition,forepart fresh water mineralization condition,buried mineralization condition.

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